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Growth of aerobic bacteria on alkali-solubilized lignite

Conference ·
OSTI ID:431603
; ; ;  [1]
  1. Idaho National Engineering Lab., Idaho Falls, ID (United States)

Coal contains a complex mixture of organic compounds, the variety of which depends on the particular type of coal. There is a general agreement that coal is composed of a macromolecular fraction and a lower-mol-wt fraction that are noncovalently associated with each other. Huttinger and Michenfelder have proposed a structural unit for the macromolecular portion of a lignite coal that comprises 2 and 3-ring fused aromatics, paraffin, terpene, cycloaliphatics, hydrocarbon bridges, several carboxyl moieties, straight-chain saturated hydrocarbons, branched-chain hydrocarbons, sulfur heterocyclics, ether linkages, alcohol groups, nitrogen heterocyclics, and chelated metals. Low-mol-wt compounds found in coal can be separated from macromolecules by extraction with organic solvents, such as tetrahydrofuran. Low-mol-wt organic compounds that have been revealed by such extractions include straight-chain (C{sub 13}-C{sub 33}), branched, and cyclic alkanes; aryl and aryl alkyl compounds with 1-6 rings; and phenolic compounds. In low-ranked coals, branched alkanes predominate over straight chain. This report describes the enrichment for, and isolation of, microorganisms that are capable of modifying lignite.

Research Organization:
Oak Ridge National Lab., TN (United States); Badger Engineers, Inc., Tampa, FL (United States); Solar Energy Research Inst., Golden, CO (United States)
OSTI ID:
431603
Report Number(s):
CONF-900512--
Country of Publication:
United States
Language:
English

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